Cold, dense, water mass originating in the Southern Ocean surrounding Antarctica
AABW is formed in the Southern Ocean from surface water cooling in polynyas.
The Antarctic bottom water (AABW) is a type of water mass in the Southern Ocean surrounding Antarctica with temperatures ranging from −0.8 to 2 °C (35 °F) and absolute salinities from 34.6 to 35.0 g/kg.[1] As the densest water mass of the oceans, AABW is found to occupy the depth range below 4000 m of all ocean basins that have a connection to the Southern Ocean at that level.[2] AABW forms the lower branch of the large-scale movement in the world's oceans through thermohaline circulation.
AABW forms near the surface in coastal polynyas along the coastline of Antarctica,[3] where high rates of sea ice formation during winter leads to the densification of the surface waters through brine rejection.[4] Since the water mass forms near the surface, it is responsible for the exchange of large quantities of heat and gases with the atmosphere.[5] AABW has a high oxygen content relative to the rest of the oceans' deep waters, but this depletes over time. This water sinks at four distinct regions around the margins of the continent and forms the AABW; this process leads to ventilation of the deep ocean, or abyssal ventilation.[6]
^Schmidt, Christina; Morrison, Adele K.; England, Matthew H. (17 June 2023). "Wind– and Sea-Ice–Driven Interannual Variability of Antarctic Bottom Water Formation". Journal of Geophysical Research: Oceans. 128 (6). Bibcode:2023JGRC..12819774S. doi:10.1029/2023JC019774. S2CID 259468175.
^"AMS Glossary of Meteorology, Antarctic Bottom Water". American Meteorological Society. Retrieved 29 June 2023.
^Portela, Esther; Rintoul, Stephen R.; Herraiz-Borreguero, Laura; Roquet, Fabien; Bestley, Sophie; van Wijk, Esmee; Tamura, Takeshi; McMahon, Clive R.; Guinet, Christophe; Harcourt, Robert; Hindell, Mark A. (December 2022). "Controls on Dense Shelf Water Formation in Four East Antarctic Polynyas". Journal of Geophysical Research: Oceans. 127 (12). Bibcode:2022JGRC..12718804P. doi:10.1029/2022JC018804. ISSN 2169-9275.
^Ohshima, Kay I.; Fukamachi, Yasushi; Williams, Guy D.; Nihashi, Sohey; Roquet, Fabien; Kitade, Yujiro; Tamura, Takeshi; Hirano, Daisuke; Herraiz-Borreguero, Laura; Field, Iain; Hindell, Mark; Aoki, Shigeru; Wakatsuchi, Masaaki (March 2013). "Antarctic Bottom Water production by intense sea-ice formation in the Cape Darnley polynya". Nature Geoscience. 6 (3): 235–240. Bibcode:2013NatGe...6..235O. doi:10.1038/ngeo1738. ISSN 1752-0908.
^Renfrew, Ian A.; King, John C.; Markus, Thorsten (June 2002). "Coastal polynyas in the southern Weddell Sea: Variability of the surface energy budget". Journal of Geophysical Research: Oceans. 107 (C6): 3063. Bibcode:2002JGRC..107.3063R. doi:10.1029/2000JC000720. ISSN 0148-0227.
^Gunn, Kathryn L.; Rintoul, Stephen R.; England, Matthew H.; Bowen, Melissa M. (June 2023). "Recent reduced abyssal overturning and ventilation in the Australian Antarctic Basin". Nature Climate Change. 13 (6): 537–544. Bibcode:2023NatCC..13..537G. doi:10.1038/s41558-023-01667-8.
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overflow water. Along its path across Earth the composition of the NADW is affected by other water masses, especially Antarcticbottomwater and Mediterranean...
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